Fire Climatology in the western United States:

Abstract. Advances in fire climatology have derived from recent studies of modern and paleoecological records. We convened a series of workshops and a conference session to report and review regional-scale findings, and these meetings led to the 10 papers in this special issue. Two papers focus on f...

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Bibliographic Details
Main Authors: Thomas W. Swetnama, R. Scott Andersonb
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.531.2717
http://www.ltrr.arizona.edu/~tswetnam/tws-pdf/SwetnamAnderson-IJWF2008.pdf
Description
Summary:Abstract. Advances in fire climatology have derived from recent studies of modern and paleoecological records. We convened a series of workshops and a conference session to report and review regional-scale findings, and these meetings led to the 10 papers in this special issue. Two papers focus on fire and climate patterns in the modern era using documentary records, four papers utilise tree rings to evaluate recent centuries of change, and four papers evaluate charcoal and pollen in lake, bog, and alluvial sediments over the Holocene. Here we summarise some of the key findings from these papers in the context of other recent fire climatology literature. These studies illustrate the value of long-term perspectives and spatial networks of fire and climate data in discovering the patterns and modes of past fire regime and climate variations. Warming temperatures and increasing drought occurrence in many regions of the world are resulting in widespread ecosys-tem impacts (ACIA 2005; IPCC 2007). One of the most dramatic ecological responses to climate change is wildfire. The impor-tance of climate in driving past, present, and future fire regimes has greatly increased the need for better understanding of fire climatology. As distinct from fire meteorology, which addresses relatively fine-scale spatial processes over short time periods (i.e.